At convergent plate borders, reverse faults exist, but at divergent plate boundaries, normal faults do. Because there is little to no vertical displacement along strike-slip faults near transform plate borders, earthquakes seldom result in tsunamis.
The majority of significant tsunamis happen near convergent plate borders when two plates are colliding. One plate is pushed under the other as the two plates contact. As a result, pressure begins to develop as the leading edge of the highest plate catches on the bottom plate.
Convergent plate boundaries are seen in subduction zones when two plates are clashing while one of the plates is in subduction zones back into the Earth. Tsunamis are frequently brought on by this particular sort of plate boundary.
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